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SPHENE , a See also:mineral consisting of See also:calcium titan-silicate, CaTiSiO5, crystallizing in the See also:monoclinic See also:system. The crystals vary considerably in See also:habit, but are generally thin and See also:wedge-shaped; hence the name sphene, from the See also:Greek a¢ v (a wedge), given by R. J. See also:Hauy in 18or. The earlier name titanite, given by M. H. See also:Klaproth in 1795, is also in See also:common use. Twinning on the ortho-pinacoid is not uncommon.
The See also:colour is See also:green, yellow, See also: As small embedded crystals, sphene has a wide See also:distribution as an See also:accessory constituent of many kinds of igneous rocks (See also:granite, See also:syenite, See also:trachyte, See also:phonolite, &c.), and also of See also:gneiss, schist and crystalline See also:limestone. Sharply-See also:developed, transparent, See also:pale green crystals are frequently associated with adularia, See also:asbestos and See also:quartz in the crystal-lined crevices of the See also:schists of the Swiss and Tyrolese See also:Alps. Large, rough and dark-coloured crystals are found at See also:Arendal and KragerS in See also:Norway, and in granular limestone at See also:Diana in New See also:York and Eganville in See also:Ontario. A greyish, compact and impure' variety of spheric, known as " leucoxene," frequently occurs in basic igneous rocks as an alteration product of See also:ilmenite and See also:rutile. (L. J. Additional information and CommentsThere are no comments yet for this article.
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